塔里木盆地塔北隆起西部巴什基奇克组层序地层及沉积演化

刘永福, 夏辉, 孙琦, 林畅松, 赵海涛, 李浩, 黄腊梅, 张知源

doi:10.11764/j.issn.1672-1926.2018.10.003

天然气地球科学 >

2019 , Vol. 30 >Issue 1: 62 - 73

DOI: https://doi.org/10.11764/j.issn.1672-1926.2018.10.003

天然气地质学

塔里木盆地塔北隆起西部巴什基奇克组层序地层及沉积演化

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1.中国石油塔里木油田分公司勘探开发研究院，新疆库尔勒 841000； 2.中国地质大学（北京）能源学院，北京 100083; 3.中国地质大学（北京）海洋学院，北京 100083

刘永福（1979-），男，山东威海人，高级工程师，硕士，主要从事沉积储层与石油地质研究.E-mail：liuyongf-tlm@petrochina.com.cn.

收稿日期: 2018-07-30

修回日期: 2018-10-13

网络出版日期: 2019-01-31

基金资助

国家科技重大专项“大型地层油气藏形成主控因素与有利区带评价”(编号：2017ZX05001-001)；国家自然科学基金重点项目“塔里木盆地古生代古构造、古地理演变与成藏效应”(编号：41130422)联合资助.

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Sequence stratigraphy and depositional evolution of the Bashijiqike Formation in the western Tabei Uplift，Tarim Basin

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1.Research Institute of Exploration and Development，PetroChina Tarim Oilfield Branch Company，Korla 841000，China；
2.School of Energy Resource，China University of Geosciences（Beijing），Beijing 100083，China；
3.School of Ocean Sciences，China University of Geosciences（Beijing），Beijing 100083，China

Received date: 2018-07-30

Revised date: 2018-10-13

Online published: 2019-01-31

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摘要

综合利用钻井、测井和地震资料，应用经典层序地层学理论，建立了塔里木盆地塔北隆起西部下白垩统巴什基奇克组层序地层格架。依据区域性不整合面、沉积相突变界面及地层叠置样式转变面，可识别出4个层序界面，将巴什基奇克组划分为由一个完整的湖平面升降旋回构成的二级层序，可进一步划分出3个三级层序，其内部可划分出低位体系域、湖侵体系域和高位体系域。通过岩心观察、测井曲线及地震资料在层序格架内识别出了扇三角洲和辫状河三角洲沉积体系，其中扇三角洲主要为退积型，辫状河三角洲为进积型和退积型2类；分析了研究区沉积体系的分布特征、演化规律及其控制因素，建立了巴什基奇克组沉积演化模式。

关键词： 层序地层; 沉积体系; 沉积演化; 巴什基奇克组; 塔北隆起

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刘永福, 夏辉, 孙琦, 林畅松, 赵海涛, 李浩, 黄腊梅, 张知源 . 塔里木盆地塔北隆起西部巴什基奇克组层序地层及沉积演化[J]. 天然气地球科学, 2019 , 30(1) : 62 -73 . DOI: 10.11764/j.issn.1672-1926.2018.10.003

Abstract

Based on comprehensive drilling，logging and seismic data，with application of classic sequence stratigraphy theory，the sequence stratigraphic framework of Early Cretaceous Bashijiqike Formation in the western Tabei Uplift of Tarim Basin was established.According to the regional unconformities，abrupt interface of sedimentary facies and the change of transforming surface of stratigraphic accumulation type，4 sequence boundaries were identified in the study area.One second-order sequences of Bashijiqike Formation in the study area were recognized，which can consist of a complete regional lake-level rise and fall cycles.The second-order sequences can be further divided into 3 third-order sequences.Each sequence was further divided into low stand system tracts，transgressive and high stand system tracts.Fan delta and braided river delta sedimentary systems are identified，based on the analysis of core observation，well logs and seismic data within sequences in the study area.The fan deltas of Bashijiqike Formation developed in the study area are mainly regressive type and the braided river deltas are progressive type and degenerate type.The distribution and evolution of depositional systems and their controlling factors in the study area are analyzed.Then，the depositional evolvement model of Bashijiqike Formation was established.

Key words： Sequence stratigraphy; Sedimentary systems; Depositional evolution; Bashijiqike Formation; Tabei Uplift

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